# How to write an isostasy equation

They then substitute density values for real rocks into their equation to derive thicknesses for average continental and oceanic crust, and apply their knowledge in order to draw a cross-section of the crust across South America.

Why is the distribution of topography on the earth bimodal? The students in the course range from first-quarter freshmen to senior engineering majors.

In each case, they work in teams of two or three and then the entire class shares their data. These papers are graded based on a rubric, also included below. The students then collect two forms of data.

Determining whether students have met the goals After the classroom activity is completed in class, students read two articles: Dec 31, Summary Hide Two students measure the density of different rock types by first measuring water displacement of the irregular pieces.

How the activity is situated in the course I use this activity in the 2nd or 3rd week of my course. They also measure the density of several different kinds of wood, and how high each kind floats in a tub of water.

This activity gives students a real, hands-on and mathematical understanding of the principle of isostasy. Details In this activity, students develop an explanation for the bimodal topography of the earth through measuring densities of rocks and wood blocks, deriving the isostasy equation, and applying their knowledge to estimate crustal thicknesses.

Skills and concepts that students must have mastered Students must be familiar with plate tectonics and earth structure, particularly the compositional and mechanical divisions of the interior of the Earth. Based on the data from the wood, they derive an equation that relates the density of the wood to the height at which the block floats in the water - the isostasy equation.

It is a stand-alone activity, but I refer back to it frequently throughout the remainder of the course. They measure the density of the most common rocks that make up oceanic crust basaltcontinental crust graniteand the mantle peridotite.

They need not be familiar with rock names or types. Details This activity begins with an exploration of a topographic map of the earth, ending with the question: Context Audience This activity is used in an introductory physical geology course entitled "Dynamic Earth".

Hide This activity was selected for the On the Cutting Edge Reviewed Teaching Collection This activity has received positive reviews in a peer review process involving five review categories.

The five categories included in the process are Scientific Accuracy Alignment of Learning Goals, Activities, and Assessments Pedagogic Effectiveness Robustness usability and dependability of all components Completeness of the ActivitySheet web page For more information about the peer review process itself, please see http: This page first made public:Chapter 3 Stress, Balance Equations, and Isostasy We deﬁne stress to consider forces acting at depths, and derive the equations of mass, linear momentum, angular momentum, and.

The heat equation is an example of what is known as a "partial differential equation." A differential equation is any equation in which a function (Temperature in time and space in this instance) is not represented directly, but via it's derivative.

ES L Lab 5 Isostasy Isostasy is a concept of considerable importance in the Earth sciences. In fact it displaced essentially all earlier beliefs about how topography is maintained and is one of From the above setup you can write the pressure balance equation thus.

Answer to Write an isostasy equation (mathematical model) that expresses how the density of the wood block compared to the density of the water.

Sep 20,  · Make an equation that expresses how the density of the wood block compared to the density of water, is related to the hight of the wood block that floats above the equilibrium.

(=x) 2. Use the average density of basalt and your isostasy equation (1st Q) to calculate how high (in km) basalt floats in the mint-body.com: Resolved.

• Which is Airy isostasy!

(w here is hr in our Airy equation) • Airy isostasy is a special case of flexure when D.

How to write an isostasy equation
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